BEACON eSpace at Jet Propulsion Laboratory >
JPL Technical Report Server >
JPL TRS 1992+ >
Please use this identifier to cite or link to this item:
|Title: ||Δ17O of Martian sulfate : assessment as a tool to recognize the impact of biological sulfur cycling on Mars.|
|Authors: ||Brunner, Benjamin|
Coleman, Max L.
|Keywords: ||mass independent isotope|
|Issue Date: ||14-Mar-2005 |
|Publisher: ||Pasadena, CA : Jet Propulsion Laboratory, National Aeronautics and Space Administration, 2005.|
|Citation: ||Lunar and Planetary Science Conference, League City, Texas, March 14-18, 2005.|
|Abstract: ||The Mars Rover-missions demonstrate that there are accessible Martian sulfate deposits (evaporites). These sedimentary rocks could indicate influence of past or present biotic processes even in the absence of traces of extraterrestrial life. We evaluate the potential of the analysis of mass independent isotope fractionation of oxygen in sulfate as a biosignature.|
|Appears in Collections:||JPL TRS 1992+|
Items in DSpace are protected by copyright, but are furnished with U.S. government purpose use rights.